The Geologic Time Scale Flashcards
Refers to the divisions of earth’s history based on life forms
Geologic Time Scale
are the largest intervals of geologic time with duration of hundreds of millions of years. The geologic time scale is divided into 4 major units
Eon
The geologic time scale is divided into 4 major units
Hadean Eon
Archean Eon
Proterozoic Eon
Phanerozoic Eon
there were fewer life forms. These life forms are more difficult to identify and the rocks have been disturbed often. An informal name given to the first three eons of the geologic time scale
precambrian
began 4.5 to 4 billion years ago. Known as the rock less eon. Except for the meteorites, no existing rocks on Earth today are from the Hadean eon. During this time, Earth was molten, and it would only solidify as it cooled.
hadean eon
began 1.5 billion years ago. during the Archean eon that single-celled organisms, such as blue-green algae, archeans, and bacteria, first appeared. It is the beginning of free oxygen in the atmosphere.
archean eon
the first era of the Archean Eon of the geologic record. Earth’s surface was dominated by volcanic activity during this era. The atmosphere consisted mainly of carbon dioxide and water vapor.
eroarchean era
The earliest confirmed evidence of life comes from this era, and Vaalbara, one of Earth’s earliest supercontinents, may have formed during this era.
paleoarchean era
the beginning of the Pongola glaciation on earth, which occurred in what is now South Africa. This was the first climate disaster on earth, as ice sheets covered areas of Swaziland and South Africa.
mesoarchean era
represents a key period in Earth’s evolution, as it recorded a transition in tectonic style, from an Early-Archean Earth dominated by episodic-overturn/stagnant-lid regime to a Proterozoic Earth in which modern- style Plate Tectonics became progressively established.
neoarchean era
began 2.5 billion years ago and ended 542 million years ago. the first continents appeared. This was also the time when continents merged into a single landmass called Rodinia. The Proterozoic eon is marked by the appearance of multicellular animals like sponges and the mass extinction of these organisms.
proterozoic eon
had given rise to crown eukaryotes, which are the ancestral organisms from which all modern eukaryotic lineages have evolved. This era is also marked by the earliest global-scale continent-continent belt collisions known.
paleoproterozoic era
are the breakup of the Columbia supercontinent, the formation of the Rodinia supercontinent, and the evolution of sexual reproduction. This era is marked by the further development of continental plates and plate tectonics.
mesoproterozoic era
is characterized by the most important climatic, tectonic and paleo - evolutionary changes in the Earth’s geological record
neoproterozoic era
The first life forms with parts, such as shells, scales, and bones and teeth, appeared during the Phanerozoic eon. The fossils of these life forms are great tools in the study of the history of the Phanerozoic eon.
phanerozoic eon